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首页> 外文期刊>Oceanography >JAPAN/EAST SEA WATER MASSES AND THEIR RELATION TO THE SEA'S CIRCULATION
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JAPAN/EAST SEA WATER MASSES AND THEIR RELATION TO THE SEA'S CIRCULATION

机译:日本/东海水质及其与海循环的关系

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摘要

The Japan/East Sea is well ventilated to the bottom through processes of sub-duction, open-ocean convection, and brine rejection from sea-ice production. The Japan/East Sea has a relatively short overturning time scale, and thus its deep- and bottom-water properties are in flux, tied to changing surface conditions with a delay of only decades. Concerns about possible anoxia in the abyss within a century or two may be ill founded based on observations of new bottom-water production. On the other hand, because sea ice is the source of deep and bottom water in the Japan/ East Sea, changes in climate that greatly reduce or eliminate sea ice in the Japan/ East Sea could have a profound impact on its abyssal waters.
机译:日本/东海通过俯冲,开阔海洋对流和海冰生产中的盐水排出过程,使底部通风良好。日本/东海的倾覆时间相对较短,因此其深水和底水属性不断变化,与不断变化的地表条件有关,仅延迟了几十年。根据对新的底水生产的观察,可能在一两个世纪之内对深渊可能发生的缺氧问题感到担忧。另一方面,由于海冰是日本/东海深层和底部水的来源,因此气候变化极大地减少或消除了日本/东海中的海冰,可能会对深海产生深远的影响。

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